
sedimentary
Limestone
Calcareous sedimentary rock (CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale; Color: beige, light gray, tan, or white; Luster: dull to earthy; Crystal structure: microcrystalline or fine-grained; Cleavage: none (conchoidal fracture); Specific gravity: 2.7
- Hardness
- 3 on Mohs scale
- Color
- beige, light gray, tan, or white
- Luster
- dull to earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: beige, light gray, tan, or white; Luster: dull to earthy; Crystal structure: microcrystalline or fine-grained; Cleavage: none (conchoidal fracture); Specific gravity: 2.7
Formation & geological history
Formed by the accumulation of skeletal fragments from marine organisms such as coral, algal, and foraminifera, as well as chemical precipitation of calcium carbonate in shallow marine environments over millions of years.
Uses & applications
Used extensively in construction (aggregate, concrete, road base), manufacturing of cement, agriculture (soil conditioning), and as a building stone.
Geological facts
Limestone can host extensive cave systems formed by the dissolution of calcium carbonate by slightly acidic groundwater. Many of the world's most famous monuments and historical buildings, including the Great Pyramids of Giza, are made of limestone.
Field identification & locations
Can be easily identified in the field by its characteristic reaction to dilute hydrochloric acid, which causes it to fizz or effervesce vigorously due to the release of carbon dioxide.
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